浙江煤山P/T之交碳同位素对有机碳埋藏的指示意义

黄俊华; 罗根明; 白晓; 汤新燕

Volume 32 Issue 6

Jun. 2007

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Article Navigation > Earth Science > 2007 > 32(6): 767-773

HUANG Jun-hua, LUO Gen-ming, BAI Xiao, TANG Xin-yan, 2007. The Organic Fraction of the Total Carbon Burial Flux Deduced from Carbon Isotopes across the Permo-Triassic Boundary at Meishan, Zhejiang Province. Earth Science, 32(6): 767-773.

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The Organic Fraction of the Total Carbon Burial Flux Deduced from Carbon Isotopes across the Permo-Triassic Boundary at Meishan, Zhejiang Province

1.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Biogeology and Environmental Geology of Ministry of Education, China University of Geosciences, Wuhan 430074, China

Received Date: 2007-08-25
Publish Date: 2007-11-25

Abstract

Abstract

By combining the carbon cycle model with the records of carbonate and organic (kerogen) carbon isotope composition, this paper presents the calculation of the fraction of organic carbon burial (f_org) of beds 23-40 at the GSSP of the Permian-Triassic boundary at Meishan, Zhejiang Province. The resulting calculation produces two episodes of f_org maxima observed to occur at beds 23-24 and 27-29, which respectively corresponds to the two episodic anoxic events indicated by the flourish of green sulfur bacteria. Two episodic f_org minima occurred at beds 25-26 and 32-34, generally coincident with the flourish of cyanobacteria (bed 26 and upper part of beds 29 to 34) as shown by the high value of 2-melthyhopanes. It appears that the f_org is related to the redox conditions, with greater f_org values observed at the reductive condition. The relationship between f_org and the total organic carbon (TOC) content was complex. The f_org value was low at some beds with high TOC content (such as bed 26), whilst high f_org values observed at some beds with low TOC content (e. g. bed 27). This association infers the important contribution of primary productivity to the TOC content. The original organic burial could be thus calculated through the configuration of the function of the primary productivity and f_org, which can be used to correct the residual TOC measured in modern time. This investigation indicates that compiling the organic-inorganic carbon isotopes with the carbon cycle model favors to understand the fraction of organic carbon burial, providing information for the reconstruction of the coupling among biota, environments and organic burial.
- carbon isotope,
- carbon cycle,
- organic burial,
- Permian-Triassic boundary

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References

Bowring, S. A., Erwin, D. H., Jin, Y. G., et al., 1998. U/Pb zircon geochronology and tempo of the end-Permianmass extinction. Science, 280 (5366): 1039-1045. doi: 10.1126/science.280.5366.1039

Cao, C. Q., Wang, W., Jin, Y. G., 2002. Carbon isotope ex-cursions across the Permian-Triassic boundary in the Meishan section, Zhejiang Province, China. Chinese Sci-ence Bulletin, 47 (13): 1125-1129. doi: 10.1360/02tb9252

Dai, J. X., Li, J., Luo, X., et al., 2005. Alkane carbon isotop-ic composition and gas sourcein giant gas field of Ordos basin. Acta Petrolei Sinica, 26 (1): 18-26 (in Chinesewith English abstract).

Gao, B., Fan, M., Liu, W. H., et al., 2005. Carbon isotopic features and genetic type of natural gas in Tahe oilfield. Oil & Gas Geology, 26 (5): 618-622 (in Chinese withEnglish abstract).

Grice, K., Gao, C., Love, G. D., et al., 2005. Photic zone eu-xinia during the Permian-Triassic superanoxic event. Science, 307: 706-709. doi: 10.1126/science.1104323

Guo, Q. J., Liu, C. Q., Strauss, H., et al., 2004. Isotopic in-vestigation of Late Neoproterozoic and Early Cambrian carbon cycle on the northern Yangtze platform, South China. Acta Geoscientica Sinica, 25 (2): 151-156 (inChinese with English abstract).

Haas, J., Demény, A., Hips, K., et al., 2007. Biotic and en-vironmental changes in the Permian-Triassic boundary interval recorded on a western Tethyan ramp in the Bükk Mts., Hungary. Global and Planetary Change, 55 (1-3): 136-154. doi: 10.1016/j.gloplacha.2006.06.010

Hayes, J. M., Strauss, H., Kauf man, A. J., 1999. The abun-dance of ¹³C in marine organic matter and isotopic frac-tionation in the global biogeochemical cycle of carbon during the past 800 Ma. Chemical Geology, 161 (1-3): 103-125. doi: 10.1016/S0009-2541(99)00083-2

Huang, X. Y., Jiao, D., Lu, L. Q., et al., 2007. The fluctua-ting environment associated with the episodic biotic cri-sis during the Permian-Triassic transition: Evidence from microbial biomarkers in Changxing, Zhejiang Prov-ice. Science in China (Series D), 50: 1052-1059. doi: 10.1007/s11430-007-0024-x

Krull, E. S., Lehrmann, D. J., Druke, D., et al., 2004. Stable carbon isotope stratigraphy across the Permian-Triassicboundary in shallow marine carbonate platforms, Nan-panjiang basin, South China. Palaeogeography, Palaeo-climatology, Palaeoecology, 204 (3-4): 297-315. doi: 10.1016/S0031-0182(03)00732-6

Kump, L. R., 1991. Interpreting carbon-isotope excursions: Strangelove oceans. Geology, 19 (4): 299-302. doi: 10.1130/0091-7613(1991)019<0299:ICIESO>2.3.CO;2

Kump, L. R., Arthur, M. A., 1999. Interpreting carbon-iso-tope excursions: Carbonates and organic matter. Chemi-cal Geology, 161 (1-3): 181-198. doi: 10.1016/S0009-2541(99)00086-8

Kump, L. P., Garrels, R. M., 1986. Modeling at mospheric O₂ in the global sedimentary redor cycle. Am. J. Sci. , 286: 337-360. doi: 10.2475/ajs.286.5.337

Li, Y. C., Zhou, Z. Z., 2002. Massive dissociation of gas hy-drate during oceanic anoxia as a cause of mass extinc-tion at the end Permian. Geology Geochemistry, 30: 57-63 (in Chinese with English abstract).

Magaritz, M., Baer, R., Baud, A., et al., 1988. The carbon-iso-tope shift at the Permian/Triassic boundary in the southern Alps is gradual. Nature, 331 (6154): 337-339. doi: 10.1038/331337a0

Magaritz, M., Krishnamurthy, R. V., Holser, W. T., 1992. Parallel trends in organic and inorganic carbon isotopes across the Permian/Triassic boundary. American Jour-nal of Science, 292 (10): 727-739. doi: 10.2475/ajs.292.10.727

McCrea, J. M., 1950. The isotopic chemistry of carbonates and a paleotemperature scale. The Journal of Chemical Physics, 18: 849-857. doi: 10.1063/1.1747785

Payne, J. L., Lehrmann, D. J., Wei, J. Y., et al., 2004. Large perturbations of the carbon cycle during recovery from the end-Permian extinction. Science, 305 (5683): 506-509. doi: 10.1126/science.1097023

Riccardi, A., Kump, L. R., Arthur, M. A., et al., 2007. Car-bon isotopic evidence for chemocline upward excursions during the end-Permian event. Palaeogeography, Palaeoclimatology, Palaeoecology, 248 (1-2): 73-81. doi: 10.1016/j.palaeo.2006.11.010

Shi, Y. Z., Hu, C. Y., Fang, N. Q., et al., 2004. Carbon iso-topic composition of organic matter in Co-rich ferro-manganese crust and its implication for paleoceanogra-phy. Earth Science—Journal of China University of Geosciences, 29 (2): 148-150 (in Chinese with Englishabstract).

Smith, R. M. H., MacLeod, K. G., 1994. Sedimentology and carbonisotope stratigraphy across the Permian-Triassic boundary in the Karoo basin, South Africa. Journal of African Earth Sciences, 27: 185-186.

Tenger, Liu, W. H., Xu, Y. C., et al., 2004. Organic carbonisotope record in marine sediment andits environmental significance—An example from Ordos basin, NW Chi-na. Petroleum Exploration and Development, 31 (5): 11-16 (in Chinese with English abstract).

Tenger, Liu, W. H., Xu, Y. C., et al., 2006. Comprehensive geochemical identification of highly evolved marine car-bonate rocks as hydrocarbon-source rocks as exempli-fied by the Ordos basin. Science in China (Series D), 49 (4): 384-396. doi: 10.1007/s11430-006-0384-7

Voigt, S., Andrew, S. G., Voigt, T., 2006. Sea-level change, car-bon cycling and palaeocli mate during the Late Cenomanian of northwest Europe: An integrated palaeoenvironmental analysis. Cretaceous Research, 27 (6): 836-858. doi: 10.1016/j.cretres.2006.04.005

Wang, C. J., Liu, Y. M., Liu, H. X., et al., 2005. Geochemi-cal significance of the relative enrichment of Pristaneand the negative excursion of δ¹³C_Pr across the Permian-Triassic Boundary at Meishan, China. Chinese Science Bulletin, 50 (19): 2213-2225. doi: 10.1007/BF03182673

Xie, S. C., Pancost, R. D., Huang, J. H., et al., 2007a. Adouble carbon isotope perturbation during the Permo/Triassic crisis. Geology, in press.

Xie, S. C., Pancost, R. D., Huang, X. Y., et al., 2007b. Mo-lecular and isotopic evidence for episodic environmental change across the Permo/Triassic boundary at Meishanin South China. Global and Planetary Change, 55 (1-3): 56-65. doi: 10.1016/j.gloplacha.2006.06.016

Xie, S. C., Pancost, R., Yin, H. F., et al., 2005. Two epi-sodes of microbial change coupled with Permo/Triassicfaunal mass extinction. Nature, 434 (7032): 494-497. doi: 10.1038/nature03396

Xu, D. Y., Yan, Z., 1993. Carbon isotope and iridium eventmarkers near the Permian/Triassic boundary in the Meishan section, Zhejiang Province, China. Paleogeogra-phy, Paleoclimatology, Paleoecology, 104 (1-4): 171-175. doi: 10.1016/0031-0182(93)90128-6

Xu, R., Gong, Y. M., Tang, Z. D., 2006. Blooming ofbacteria and algae: Possible killer of Devonian Frasnian-Famennian mass extinction? Earth Science—Journal of China University of Geosciences, 31 (6): 787-797 (inChinese with English abstract).

Xu, Y. C., Shen, P., Liu, W. H., et al., 2001. Isotopic composi-tion characteristics and identification of immature and low-mature oils. Chinese Science Bulletin, 46 (22): 1923-1929. doi: 10.1007/BF02901173

Yin, H. F., Zhang, K. X., Tong, J. N., et al., 2001. The Global Stratotype Section and Point (GSSP) of the Per-mian-Triassic boundary. Episodes, 24 (2): 102-114. doi: 10.18814/epiiugs/2001/v24i2/004

Zhang, F., Feng, Q. L., He, W. H., et al., 2006. Multidisci-plinary stratigraphy across the Permian-Triassic bound-ary in deep-water environment of the Dongpan section, South China. Norwegian Journal of Geology, 125-131.

Zhang, S. C., Wang, R. L., Jin, Z. J., et al., 2006. The rela-tionship between the Cambrian-Ordovician high-TOC source rock development and paleoenvironment varia-tions in the Tarim basin, Western China: Carbon and oxygen isotope evidence. Acta Geologica Sinica, 80 (3): 459-466 (in Chinese with English abstract).

戴金星, 李剑, 罗霞, 等, 2005. 鄂尔多斯盆地大气田的烷烃气碳同位素组成特征及其气源对比. 石油学报, 26 (1): 18-26. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB200501003.htm

高波, 范明, 刘文汇, 等, 2005. 塔河油田天然气的碳同位素特征及其成因类型. 石油与天然气地质, 26 (5): 618-622. doi: 10.3321/j.issn:0253-9985.2005.05.010

郭庆军, 刘丛强, Strauss, H., 等, 2004. 晚震旦世至早寒武世扬子地台北缘碳同位素研究. 地球学报, 25 (2): 151-156. doi: 10.3321/j.issn:1006-3021.2004.02.010

李玉成, 周忠泽, 2002. 华南二叠纪末缺氧海水中的有毒气体与生物绝灭事件. 地质地球化学, 30: 57-63. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDQ200201009.htm

史跃中, 胡超涌, 方念乔, 等, 2004. 富钴结壳中有机碳同位素组成特征及其古海洋意义. 地球科学——中国地质大学学报, 29 (2): 148-150. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200402004.htm

腾格尔, 刘文汇, 徐永昌, 等, 2004. 海相沉积有机质的碳同位素记录及其环境意义——以鄂尔多斯盆地为例. 石油勘探与开发, 31 (5): 11-16. doi: 10.3321/j.issn:1000-0747.2004.05.003

徐冉, 龚一鸣, 汤中道, 2006. 菌藻类繁盛: 晚泥盆世大灭绝的疑凶?地球科学——中国地质大学学报, 31 (6): 787-797. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200606006.htm

张水昌, Wang, R. L., 金之钧, 等, 2006. 塔里木盆地寒武纪-奥陶纪优质烃源岩沉积与古环境变化的关系: 碳氧同位素新证据. 地质学报, 80 (3): 459-466. doi: 10.3321/j.issn:0001-5717.2006.03.020

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The Organic Fraction of the Total Carbon Burial Flux Deduced from Carbon Isotopes across the Permo-Triassic Boundary at Meishan, Zhejiang Province

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